Environmental Engineering Reference
In-Depth Information
3.12 Chapter Summary
After reading this chapter, the reader may come away with the thought that wetland
hydrology is complex but there are many different approaches and tools that can be
used, or that quantifying hydrologic fluxes in wetland settings is difficult and
fraught with error. Either impression would be correct. Perhaps the most important
conclusion is that the pursuit of parallel lines of evidence, using multiple methods
for achieving the same goals, will lead to a better understanding of these complex
processes and a more accurate assessment of the various hydrologic components
that constitute the hydrologic setting of a wetland. Armed with the numerous
methods at our disposal, and knowledge of the various sources and magnitudes of
error associated with each approach, the wetland hydrologist can feel comfortable
in pursuing quantification of the various hydrological components with a judicious
selection of methods appropriate to the goals and budget associated with the
investigation.
References
Abtew W (2001) Evaporation estimation for Lake Okeechobee in south Florida. J Irrig Drain Eng
127:140-147
Adams DD (1994) Sediment pore water sampling. In: Mudrock A, MacKnight (eds) Handbook of
techniques for aquatic sediments sampling. Lewis Publishers, Boca Raton
Allan MA (2004) Manual for the GAW precipitation chemistry programme: guidelines, data
quality objectives and standard operation procedures. World Meteorological Organization
Global Atmosphere Watch No. 160:170
Allen RG, Pereira LS, Raes D, Smith M (1998) Crop evapotranspiration - guidelines for computing
crop water requirements. Food and Agricultural Organization of the United Nations FAO
Irrigation and drainage paper 56:328
Belanger TV, Kirkner RA (1994) Groundwater/surface water interaction in a Florida augmentation
lake. Lake Reserv Manag 8:165-174
Bouwer H (1989) The Bouwer and Rice slug test - an update. Ground Water 27:304-309
Bouwer H, Rice RC (1976) A slug test for determining hydraulic conductivity of unconfined
aquifers with completely or partially penetrating wells. Water Resour Res 12:423-428
Brooks R (2009) Potential impacts of global climate change on the hydrology and ecology of
ephemeral freshwater systems of the forests of the northeastern United States. Clim Chang
95:469-483
Brunsell NA, Ham JM, Owensby CE (2008) Assessing the multi-resolution information content of
remotely sensed variables and elevation for evapotranspiration in a tall-grass prairie environ-
ment. Remote Sens Environ 112:2977-2987
Brutsaert WH, Stricker H (1979) An advection-aridity approach to estimate actual regional
evapotranspiration. Water Resour Res 15:443-450
Carr MR, Winter TC (1980) An annotated bibliography of devices developed for direct measurement
of seepage. U.S. Geological Survey Open-File Report 80-344:38
Choi J, Harvey JW (2000) Quantifying time-varying ground-water discharge and recharge in
wetlands of the northern Florida Everglades. Wetlands 20:500-511
Conly FM, Su M, van der Kamp G, Millar JB (2004) A practical approach to monitoring water
levels in prairie wetlands. Wetlands 24:219-226
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